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| 1 | 青藏高原中东部过去2485年以来温度变化的树轮记录显示文摘通过青藏高原东北部现生活树与墓葬古木相衔接,利用树轮宽度重建了这一地区过去2485a以来的年均温度变化序列.这个温度序列所揭示的气候历史表明序列中有4个时期的温度高于或接近1970~2000AD的平均温度.348~413AD出现过一次快速的由寒冷到温暖的气候突变事件,文中称之为'东晋事件'.计算表明,高原中东部长时间尺度温度变化不仅反映了中国中北地区,同时也响应了北半球的温度变化.在过去2485a里,中国绝大部分朝代的灭亡都与该温度序列的低温时期相对应.此外,与中国其他地区的温度记录相比较,高原中东部在1950年代之后升温幅度更高一些. | 刘禹 安芷生 Hans W. Linderholm Deliang Chen 宋慧明 蔡秋芳 孙军艳 田华 | 2009 | 中国科学(D辑)2009，，2： | 64 |
| 2 | Linking atmospheric pollution to cryospheric change in the Third Pole region: current progress and future prospects显示文摘The Tibetan Plateau and its surroundings are known as the Third Pole(TP). This region is noted for its high rates of glacier melt and the associated hydrological shifts that affect water supplies in Asia. Atmospheric pollutants contribute to climatic and cryospheric changes through their effects on solar radiation and the albedos of snow and ice surfaces; moreover, the behavior and fates within the cryosphere and environmental impacts of environmental pollutants are topics of increasing concern. In this review, we introduce a coordinated monitoring and research framework and network to link atmospheric pollution and cryospheric changes(APCC) within the TP region. We then provide an up-to-date summary of progress and achievements related to the APCC research framework, including aspects of atmospheric pollution’s composition and concentration, spatial and temporal variations, trans-boundary transport pathways and mechanisms, and effects on the warming of atmosphere and changing in Indian monsoon, as well as melting of glacier and snow cover. We highlight that exogenous air pollutants can enter into the TP’s environments and cause great impacts on regional climatic and environmental changes. At last, we propose future research priorities and map out an extended program at the global scale. The ongoing monitoring activities and research facilitate comprehensive studies of atmosphere–cryosphere interactions, represent one of China’s key research expeditions to the TP and the polar regions and contribute to the global perspective of earth system science. | Shichang Kang Qianggong Zhang Yun Qian Zhenming Ji Chaoliu Li Zhiyuan Cong Yulan Zhang Junming Guo Wentao Du Jie Huang Qinglong You Arnico K.Panday Maheswar Rupakheti Deliang Chen Orjan Gustafsson Mark H.Thiemens Dahe Qin | 2019 | National Science Review2019，6，4： | 35 |
| 3 | 青藏高原河川径流变化及其影响研究进展显示文摘青藏高原被称为世界'第三极',又有'亚洲水塔'之称,对其周边地区的水文和气候系统有重要影响.青藏高原是亚洲许多大河的发源地,其冰川与河川径流变化影响到周边数十亿人口.本文介绍了青藏高原河川径流观测现状,回顾了青藏高原河川径流变化研究. 20世纪50年代至21世纪初,黄河源区年径流呈减少趋势、长江源区年径流呈微弱增加趋势,青藏高原其他江河源区的年径流没有显著的变化趋势.黄河上游、澜沧江上游、沱沱河及拉萨河源区的春季径流有增加趋势.未来气候变化情景下,随着降水和冰雪融水增加,青藏高原大部分河流源区径流增加,洪水等极端水文事件发生更加频繁.青藏高原河流源区水文气象观测资料稀缺,是河川径流变化及其影响研究的重大挑战.青藏高原水文研究亟需结合最新观测与模拟技术,提高水循环观测与模拟能力,深入认识青藏高原河川径流复杂性及其变化规律,为径流变化的影响评估及其应对提供科技支撑. | 汤秋鸿 兰措 苏凤阁 刘星才 孙赫 丁劲 王磊 冷国勇 张永强 桑燕芳 方海燕 张士锋 韩冬梅 刘小莽 贺莉 徐锡蒙 唐寅 Deliang Chen | 2019 | 科学通报2019，64，27： | 39 |
| 4 | Spatial and temporal variations and controlling factors of potential evapotranspiration in China:1956-2000显示文摘Based on the climatic data of 580 stations in China during 1956 and 2000, potential evapotranspiration are calculated using the Penman-Monteith Method recommended by FAO. The spatial and temporal distributions of the potential evapotranspiration over China and the temporal trends of the regional means for 10 major river basins and whole China are analyzed. Through a partial correlation analysis, the major climate factors which affect the temporal change of the potential evapotranspiration are analyzed. Major results are drawn as follows: 1) The seasonal and annual potential evapotranspiration for China as a whole and for most basins show decline tendencies during the past 45 years; for the Songhua River Basin there appears a slightly increasing trend. 2) Consequently, the annual potential evapotranspirations averaged over 1980-2000 are lower than those for the first water resources assessment (1956-1979) in most parts of China. Exceptions are found in some areas of Shandong Peninsula, western and middle basins of the rivers in Southwest China, Ningxia Hui Autonomous Region as well as the source regions of the Yangtze and Yellow rivers, which may have brought about disadvantages to the exploration and utilization of water resources. 3) Generally, sunshine duration, wind speed and relative humidity have greater impact on the potential evapotranspiration than temperature. Decline tendencies of sunshine duration and/or wind speed in the same period appear to be the major causes for the negative trend of the potential evapotranspiration in most areas. | GAO Ge CHEN Deliang REN Guoyu CHEN Yu LIAO Yaoming | 2006 | Journal of Geographical Sciences2006，16，1： | 34 |
| 5 | 1961-2004年海河流域夏季逐时降水变化趋势显示文摘利用海河流域21个气象站1961~2004年夏季逐时降水资料,分析海河流域夏季极端小时降水、降水过程雨强的长期变化趋势.结论如下:海河流域夏季总降水量和总降水小时数以及长、短历时降水量均呈减少趋势,但短历时降水量占总降水量的比重呈增加趋势.短历时降水过程平均雨强和峰值雨强均呈增加趋势,到达峰值雨强的时刻略有提前,可能与这一地区地表气温上升,而对流层中上层气温下降,引起上下层热力差异加剧有关.长历时降水量与东亚夏季风指数的相关系数达到0.63.尽管近40年长历时降水量显著减少,但长历时降水过程平均雨强和峰值雨强,以及≥10mm/h的极端小时降水在流域的东西部呈相反的变化趋势,即东部呈减少趋势,西部呈增加趋势.这一差异可能与流域东西部显著的地形差异有关. | 殷水清 高歌 李维京 CHEN DeLiang 郝立生 | 2012 | 中国科学:地球科学2012，42，2： | 33 |
| 6 | Diurnal Variations of Summer Precipitation in the Beijing Area and the Possible Effect of Topography and Urbanization显示文摘The present study examined the diurnal variations of summer precipitation in the Beijing area by using subdaily precipitation and wind observations. A combined effect of topography and urbanization on the characteristics of diurnal variations was suggested. It was shown that stations located in the plain areaexhibited typical night rain peaks, whereas those in the mountainous area exhibited clear afternoon peaks ofprecipitation diurnal variations. The precipitation peaks were associated with wind fields around the Beijing area, which were found to be highly modulated by mountain-valley circulation and urban-country circulation.The lower-tropospheric wind exhibited a clear diurnal shift in its direction from north at 0800 LST to southat 2000 LST, which reflected mountain-valley circulation. The transitions from valley to mountain windand the opposite generally happened after sunset and sunrise, respectively, and both occurred earlier for thestations located closer to mountains. By comparing the diurnal variations of precipitation at stations in anortheast suburb, an urban area, and a southwest suburb, it was revealed that the northeast suburb grouphad the highest normalized rainfall frequency, but the southwest group had the lowest from late afternoon tolate evening. On the contrary, in the early morning from about 0200 to 1000 LST, the southwest group andurban group had the highest normalized rainfall frequency. This pattern might originate from the combined effects of mountain-valley topography and urbanization. | 殷水清 李维京 Deliang CHEN Jee-Hoon JEONG 郭文利 | 2011 | Advances in Atmospheric Sciences2011，28，4： | 26 |
| 7 | Spatial Interpolation of Daily Precipitation in China:1951-2005显示文摘Climate research relies heavily on good quality instrumental data; for modeling efforts gridded data are needed. So far, relatively little effort has been made to create gridded climate data for China. This is especially true for high-resolution daily data. This work, focuses on identifying an accurate method to produce gridded daily precipitation in China based on the observed data at 753 stations for the period 1951-2005. Five interpolation methods, including ordinary nearest neighbor, local polynomial, radial basis function, inverse distance weighting, and ordinary kriging, have been used and compared. Cross-validation shows that the ordinary kriging based on seasonal semi-variograms gives the best performance, closely followed by the inverse distance weighting with a power of 2. Finally the ordinary kriging is chosen to interpolate the station data to a 18 km× 18 km grid system covering the whole country. Precipitation for each 0.5°×0.5° latitude-longitude block is then obtained by averaging the values at the grid nodes within the block. Owing to the higher station density in the eastern part of the country, the interpolation errors are much smaller than those in the west (west of 100°E). Excluding 145 stations in the western region, the daily, monthly, and annual relative mean absolute errors of the interpolation for the remaining 608 stations are 74%, 29%, and 16%, respectively. The interpolated daily precipitation has been made available on the internet for the scientific community. | Deliang CHEN Tinghai OU Lebing GONG ChongYu XU 李维京 Chang—Hoi HO 钱维宏 | 2010 | Advances in Atmospheric Sciences2010，27，6： | 20 |
| 8 | Statistical Downscaling Based on Dynamically Downscaled Predictors: Application to Monthly Precipitation in Sweden显示文摘A prerequisite of a successful statistical downscaling is that large-scale predictors simulated by the General Circulation Model (GCM) must be realistic. It is assumed here that features smaller than the GCM resolution are important in determining the realism of the large-scale predictors. It is tested whether a three-step method can improve conventional one-step statistical downscaling. The method uses predictors that are upscaled from a dynamical downscaling instead of predictors taken directly from a GCM simulation. The method is applied to downscaling of monthly precipitation in Sweden. The statistical model used is a multiple regression model that uses indices of large-scale atmospheric circulation and 850-hPa specific humidity as predictors. Data from two GCMs (HadCM2 and ECHAM4) and two RCM experiments of the Rossby Centre model (RCA1) driven by the GCMs are used. It is found that upscaled RCA1 predictors capture the seasonal cycle better than those from the GCMs, and hence increase the reliability of the downscaled precipitation. However, there are only slight improvements in the simulation of the seasonal cycle of downscaled precipitation. Due to the cost of the method and the limited improvements in the downscaling results, the three-step method is not justified to replace the one-step method for downscaling of Swedish precipitation. | Cecilia HELLSTROM Deliang CHEN | 2003 | Advances in Atmospheric Sciences2003，20，6： | 18 |
| 9 | 以树轮宽度重建公元1558年以来华山5-6月平均温度及20世纪中后期升温显示文摘通过对秦岭东端华山地区油松树木年轮宽度序列的分析研究,探讨了华山地区油松对气候环境响应的敏感性,结果表明在华山地区油松对气温和降水的响应均高于华山松,与5~6月平均温度相关较高,且通过了0.01显著性信度检验。在此基础上,我们重建了华山地区1558~2006年间5~6月的平均温度,重建序列的方差解释量达到41%。结果显示:华山过去449年中,大部分年份5~6月平均温度在平均值附近波动,变幅不大;重建序列可与秦岭南五台5~7月温度序列进行良好对比,其年际间相关系数达到了0.49(N=246,p<0.0001)。华山地区20世纪20~30年代初的暖期略偏低;20世纪30年代中期至50年代是整个重建时段中低温持续时间较长的时段;20世纪60年代之后,气温波动平缓;从20世纪70年代开始快速升温,对全球变暖有较强响应。 | 刘禹 田沁花 宋慧明 孙军艳 Hans W.Linderholm Deliang Chen 蔡秋芳 他维媛 雷莺 | 2009 | 第四纪研究2009，29，5： | 16 |
| 10 | Surface energy budget diagnosis reveals possible mechanism for the different warming rate among Earth’s three poles in recent decades显示文摘With the introduction of the‘‘Third Pole'[1],the Arctic,Antarctic,and Tibetan Plateau(TP)can be collectively referred to as the‘‘three poles of the Earth'.The cryosphere is an important component of the climate system because of its effect on Earth’s surface albedo and its role in reducing the amount of heat exchanged between the atmosphere and ocean or land(2)As the dominant parts of the cryosphere,the Arctic,Antarctic,and TP are pivotal and sensitive areas of global climate change.Global warming will weaken the inherent stability of the cryosphere,such as its ice shelves,glaciers and permafrost[3,4]. | Kailun Gao Anmin Duan Deliang Chen Guoxiong Wu | 2019 | Science Bulletin2019，64，16： | 16 |
| 11 | 第三极西风和季风主导流域源区降水呈现不同梯度特征显示文摘利用位于第三极东南部受季风主导的长江、黄河、澜沧江、怒江上游和雅鲁藏布江流域,以及位于西部受西风主导的叶尔羌河、印度河、阿姆河和锡尔河上游流域源区256个气象站的降水数据,分析了各流域降水随海拔变化的梯度关系;基于ERA5数据,通过分析水汽含量、对流有效势能和抬升凝结高度与各流域内海拔的变化关系,探讨了不同气候系统主导的流域呈现不同梯度特征的原因;通过水文模型模拟径流反向验证降水梯度校正方法在推算高海拔山区降水时的可行性.结果表明:(1)位于季风区的长江上游、黄河上游、澜沧江、怒江和雅鲁藏布江流域降水随海拔增加而降低(17~128 mm/100 m),地形效应仅在小尺度呈现;西风主导的叶尔羌河、印度河、阿姆河和锡尔河上游流域降水随海拔增加而增加(5~64 mm/100 m),地形效应明显.(2)ERA5与气象站观测降水数据在不同流域源区表现出一致的降水梯度特征.季风区流域降水随海拔增加而减少,主要由水汽含量随海拔增加而减少所致,地形效应在局地尺度依然有所反映;西风区流域降水随海拔增加而增加,主要受抬升凝结高度降低和对流有效势能增加的影响.(3)陆面水文模型反向验证结果表明,在降水地形效应明显的流域,对低海拔站点降水进行地形校正是提高通过降水变率推算高海拔区域降水可靠性、提高水文模拟精度的一个有效途径.研究结果对第三极流域高海拔山区降水数据的地形校正有参考价值;对第二次青藏高原综合科学考察中降水观测的选点有指导意义. | 孙赫 苏凤阁 黄敬恒 姚檀栋 罗毅 Deliang Chen | 2020 | 科学通报2020，65，1： | 13 |
| 12 | Long-term precipitation change by hourly data in Haihe River Basin during 1961–2004显示文摘Hourly summer precipitation data recorded at 21 stations during 1961-2004 in the Haihe River Basin in North China were analyzed. The results show that the precipitation frequency and amount and the morning peak mainly relating to long-duration rainfall events decreased during this period, whereas the normalized afternoon peak mainly relating to short-duration events increased, which may suggest that the proportion of short-duration rainfall has increased as the total summer rainfall has decreased. For short-duration events, the mean intensity and peak intensity increased at most stations and the time to peak intensity decreased, which may be attributable to the higher thermal contrast between the warmer lower surface and cooler upper level. In the case of long-duration events, the total amount was significantly correlated with the East Asian summer monsoon index for the period 1961-2001 (correlation coefficient of 0.63). Although the total amount of rainfall in long-duration events decreased in the basin, the mean intensity and peak intensity, as well as the extreme hourly precipitation, increased in the western basin and decreased in the eastern basin. | YIN ShuiQing GAO Ge LI WeiJing CHEN DeLiang HAO LiSheng | 2011 | Science China Earth Sciences2011，54，10： | 12 |
| 13 | Trends in Graded Precipitation in China from 1961 to 2000显示文摘从 1961 ~ 2000 在中国在 576 个车站观察的每日的降水率被分类进紧张的六个等级,包括踪迹(没有数量) ,细微(⩽
1 公里 d −1), 小、大、重、很重。最后四一起分级组成所谓的有效降水量(>
1 公里 d −1) 。空间分发和分级的降水天的时间的趋势被检验。在踪迹降水天内的一个减少的趋势为中国的全部被观察,除了在在长江的中间的节的南方的几个地点,当在细微降水天内的一个减少的趋势仅仅出现在东方中国时。减少的趋势并且内部踪迹降水天的年度可变性在为一样的时期的中国与温暖的趋势和相应温度可变性一致,显示一个可能的角色在云体过程由增加的表面气温玩了。为有效降水量天,当一个增加的趋势被作出对有利的裁决时,一个减少的趋势沿着黄河山谷并且为长江和西南中国的中间的活动范围被观察 Xinjiang,东方西藏的高原,东北中国和东南中国。为中间降低的黄河山谷的有效降水量天的减少的趋势和为更低的长江山谷的增加的趋势很可能在华东被连接到异常季风循环。到在有效降水量的趋势的最重要的贡献者取决于担心的区域。 | 符娇兰 钱维宏 林祥 Deliang CHEN | 2008 | Advances in Atmospheric Sciences2008，25，2： | 11 |
| 14 | Using Statistical Downscaling to Quantify the GCM-Related Uncertainty in Regional Climate Change Scenarios: A Case Study of Swedish Precipitation显示文摘有在地区性的气候变化情形的不确定性的很多来源。当统计 downscaling 被用来获得地区性的气候变化情形时,不确定性可以在使用的模型,统计模型的技巧,和强迫的情形用于世界气候模型的世界气候从不确定性发源。与世界气候模型联系的不确定性能被基于一套不同世界气候模型在预言者并且在 downscaled 气候变化情形检验差别评估。什么时候标准化了象 CoupledModel Intercomparison 工程(CMIP2 ) 的第二个阶段那样的世界气候模型模拟,被使用,在 downscaled 变量的差别主要在模仿的气候在气候模型和自然可变性反映差别。Itis 建议估计的传播能作为与世界气候模型联系的不确定性的一项措施被拿。建议方法在瑞典在地区性的降水变化情形被用于评价 ofglobal-climate-model-related 不确定性。尽管在降水的变化的可观的传播存在,基于在整个瑞典的年度降水有全面增加的 17 世界气候模型表演源于统计 downscaling。一般增加能被归因于增加的 large-scaleprecipitation 和提高的偏午。估计的不确定性将近独立于区域。然而,有季节的依赖。为冬季的估计显示出信心的高水平,当为夏天的估计最不出现时。 | Deliang CHEN Christine ACHBERGER Jouni R■IS■NEN Cecilia HELLSTRM | 2006 | Advances in Atmospheric Sciences2006，23，1： | 9 |
| 15 | Preparation,Microstructure and Properties of NiO-Cr_2O_3-TiO_2 Infrared Radiation Coating显示文摘The spherical agglomerated particles were fabricated by spray drying with the powders of NiO,Cr2O3 and TiO2.Plasma spray power,which has good property of flowability,was acquired by heat treatment from the particles at 1200-C in the reducing atmosphere.Dark and uniform coating of More than 50μm thick was deposited on the copper sheet substrate by plasma spraying.It is found that the infrared normal total emissivity of the coating is up to 0.91 at 600-C by infrared radiation testing.The X-ray diffraction analysis shows that the formation of(Cr0.88Ti0.12)2O3 and spinel structural NiCr2O4 in the coating is the main reason for high effcient infrared radiation,and the phase structure and performance of coating is favorable under the thermal cycle between room temperature and 600-C. | Wu Chen Weiping Ye Xudong Cheng Wei Duan Fang Mao Deliang Li | 2009 | Journal of Materials Science & Technology2009，25，5： | 8 |
| 16 | Strong link between large tropical volcanic eruptions and severe droughts prior to monsoon in the central Himalayas revealed by tree-ring records显示文摘Large tropical volcanic eruptions can cause short-term global cooling. However, little is known whether large tropical volcanic eruptions, like the one in Tambora/Indonesia in 1815, cause regional hydroclimatic anomalies. Using a tree-ring network of precisely dated Himalayan birch in the central Himalayas, we reconstructed variations in the regional pre-monsoon precipitation back to 1650 CE. A superposed epoch analysis indicates that the pre-monsoon regional droughts are associated with large tropical volcanic eruptions, appearing to have a strong influence on hydroclimatic conditions in the central Himalayas. In fact, the most severe drought since 1650 CE occurred after the Tambora eruption. These results suggest that dry conditions prior to monsoon in the central Himalayas were associated with explosive tropical volcanism. Prolonged La Ni?a events also correspond with persistent pre-monsoon droughts in the central Himalayas. Our results provide evidence that large tropical volcanic eruptions most likely induced severe droughts prior to monsoon in the central Himalayas. | Eryuan Liang Binod Dawadi Neil Pederson Shilong Piao Haifeng Zhu Shalik Ram Sigdel Deliang Chen | 2019 | Science Bulletin2019，64，14： | 8 |
| 17 | 人为气溶胶排放导致最近80年东亚夏季风在过去四个世纪以来空前减弱显示文摘亚洲夏季风(Asian Summer Monsoon,ASM)对亚洲数十亿人口的生存、亚洲生态系统和生物多样性的分布、以及农业生产(粮食安全)和工业活动影响严重。因此了解ASM过去时空变化及其动力学过程对陆地生态系统、水资源、森林和景观研究至关重要。近几十年,器测记录显示以降水量为代表的ASM强度一直在减弱,但这一减弱趋势的起始时间和动力学过程尚不清楚。为此,第一次集成了ASM西部-中部边缘带10个对降水敏感的树木年轮宽度年表,重建了公元1566年以来反映ASM强度变化的降水序列。重建结果不仅捕捉到了ASM过去4个世纪以来强弱变化历史,也反映出历史上蝗灾与弱季风的关联。特别是发现了最近80年具有过去448年中前所未有的、最为强烈的、显著且持续时间最长的ASM强度减弱趋势。这一减弱趋势与在温室效应影响下ASM本该增强的预期大相庭径。耦合气候模型实验表明,北半球人为硫酸盐气溶胶排放的逐渐增加,对ASM减弱起了决定性作用。 | 刘禹 蔡文炬 孙长峰 宋慧明 Kim MCobb 李建平 Steven WLeavitt 吴立新 蔡秋芳 刘若时 Benjamin Ng Paolo Cherubini Ulf Büntgen 宋怡 王国建 雷莺 晏利斌 李强 马永永 方丛羲 孙军艳 李旭祥 Deliang Chen Hans WLinderholm | 2019 | 地球环境学报2019，10，6： | 7 |
| 18 | Statistical Downscaling of Summer Temperature Extremes in Northern China显示文摘Two approaches of statistical downscaling were applied to indices of temperature extremes based on percentiles of daily maximum and minimum temperature observations at Beijing station in summer during 1960-2008. One was to downscale daily maximum and minimum temperatures by using EOF analysis and stepwise linear regression at first, then to calculate the indices of extremes; the other was to directly downscale the percentile-based indices by using seasonal large-scale temperature and geo-potential height records. The cross-validation results showed that the latter approach has a better performance than the former. Then, the latter approach was applied to 48 meteorological stations in northern China. The cross-validation results for all 48 stations showed close correlation between the percentile-based indices and the seasonal large-scale variables. Finally, future scenarios of indices of temperature extremes in northern China were projected by applying the statistical downscaling to Hadley Centre Coupled Model Version 3 (HadCM3) simulations under the Representative Concentration Pathways 4.5 (RCP 4.5) scenario of the Fifth Coupled Model Inter-comparison Project (CMIP5). The results showed that the 90th percentile of daily maximum temperatures will increase by about 1.5℃, and the 10th of daily minimum temperatures will increase by about 2℃ during the period 2011-35 relative to 1980-99. | 范丽军 Deliang CHEN 符淙斌 严中伟 | 2013 | Advances in Atmospheric Sciences2013，30，4： | 7 |
| 19 | Tumor-homing peptide-based NIR-II probes for targeted spontaneous breast tumor imaging显示文摘Fluorescence imaging in the second near-infrared window(NIR-Ⅱ,1000-1700 nm)is a promising modality for real-time imaging of cancer and image-guided surgery with superior in vivo optical properties.So far,very few NIR-Ⅱfluorophores have been reported for in vivo biomedical imaging of chemically-induced spontaneous breast carcinoma.Herein,a NIR-Ⅱfluorescent probe CH1055-F3 with the nucleolin-targeted tumor-homing peptide F3 was demonstrated to prefe rentially accumulate in 4 T1 tumors.More importantly,CH1055-F3 exhibited specific NIR-Ⅱsignals with high spatial and temporal resolution,strong tumor uptake,and remarkable NIR-Ⅱimage-guided surgery in dimethylbenzanthracene(DMBA)-induced spontaneous breast tumor rats.This report presents the first tumor-homing peptide-based NIR-Ⅱprobe to diagnose transplantable and spontaneous breast tumors by the active targeting. | Hui Zhou Shanshan Li Xiaodong Zeng Mengxian Zhang Lin Tang Qianqian Li Deliang Chen Xianli Meng Xuechuan Hong | 2020 | Chinese Chemical Letters2020，31，6： | 6 |
| 20 | A comparative analysis of nebkhas in central Tunisia and northern Burkina Faso显示文摘 | Anna Tengberg Deliang Chen | 1998 | Geomorphology1998，，2： | 5 |
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